Isentropic analysis is a common and effective way to diagnose horizontal and vertical motion of the atmosphere, the combination of 3D visualization feature of the IDV and the isentropic analysis helps us better visualize the dynamic and stability of weather phenomenons.
Edit→Remove All Displays and Data menu item
or the
icon in the toolbar to clear them out.
Fields panel open the 3D grid node and Derived node,
scroll down the Derived node and select Potential Temperature IsoSurface.
Displays open Constant Theta Surface Height Plan View node, and
select Isentropic Topography and press
Create Display
OK button to create the display.
Fields panel open the 3D grid node and Derived node,
scroll down the Derived node and select Potential Temperature IsoSurface Scalar Analysis.
Displays open 3D Theta Surface node, and
select Contours Over Constant Theta Surface and press
Create Display
Ok button, a dialog will pop up to allow you to select the
Parameter field. From the dialog, expand the 3D grid node and select
the Temperature@Isobaric surface field and click the OK button.
Fields panel open the 3D grid node and Derived node,
scroll down the Derived node and select Potential Temperature IsoSurface Vector Analysis.
Displays open Constant Theta Surface Flow Displays node, and
select Vectors Colored by Speed over Theta Surface and press
Create Display
Ok button, a dialog will pop up to allow you to select the
voctor field. From the dialog, expand the 3D grid node and
the Derived node and select the True Wind vectors field and
click the OK button.
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